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Title:
Compressional tectonics : plate convergence to mountain building/ editors, Elizabeth J. Catlos, İbrahim Çemen.
Publisher:
American Geophysical Union ;
Copyright Date:
2023
Description:
x, 334 : illustrations, maps (mostly color) ; 29 cm.
Subject:
Plate tectonics.
Convergent margins.
Subduction zones.
Orogeny.
Other Authors:
Catlos, Elizabeth J., 1971- https://id.loc.gov/authorities/names/no2013038323 editor.
Çemen, Ibrahim, 1951- https://id.loc.gov/authorities/names/no2010139607 editor.
American Geophysical Union, https://id.loc.gov/authorities/names/n79023191 publisher.
Notes:
Includes bibliographical references and index.
Summary:
"Tectonism has affected Earth's climate, geomorphology, magmatism, geochemistry, sedimentary environments, and economic resources throughout its geologic evolution. This makes tectonics a core subdiscipline in Earth sciences. Webster's dictionary defines plate tectonics as: "a theory in geology: the lithosphere of the earth is divided into a small number of plates which float on and travel independently over the mantle and much of the earth's seismic activity occurs at the boundaries of these plates." However, plate tectonics is more than just a theory; it is overwhelmingly accepted as the Unifying Theory of Earth Sciences because all aspects of Earth Sciences can be explained within the framework of plate tectonics. Earth's crust is divided into major plates and microplates, interacting with each other along divergent (extensional), convergent (compressional), and transform (strike-slip) plate boundaries. Within the last forty years, Earth sciences have made tremendous advances in our understanding of plate tectonics processes along these three different types of plate boundaries"-- Provided by publisher.
Series:
Geophysical monograph series ; 277
Tectonic processes: a global view ; volume 1
ISBN:
9781119773849
1119773849
OCLC:
(OCoLC)1385175798
LCCN:
2022054054
Locations:
USUX851 -- Iowa State University - Parks Library (Ames)
OVUX522 -- University of Iowa Libraries (Iowa City)

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